
mineral
Banded Agate
Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: White, cream, and yellow banding, Luster: Waxy to vitreous, Crystal System: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.58-2.64
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: White, cream, and yellow banding, Luster: Waxy to vitreous, Crystal System: Trigonal (microcrystalline), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.58-2.64
Formation & geological history
Formed primarily in volcanic or metamorphic environments when silica-rich groundwater fills cavities (vesicles) in lava or other rock. The characteristic banding is created by successive layers of silica deposition over many years.
Uses & applications
Commonly used for lapidary work, jewelry, stone carvings, bookends, and as healing stones in metaphysical practices. Industrially used for mortar and pestle sets because of its hardness.
Geological facts
The name 'Agate' originates from the Achates River in Sicily. Each agate specimen is unique due to the specific mineral impurities present during its formation cycle.
Field identification & locations
Identify in the field by looking for translucent edges, waxy luster, and concentric banding. Commonly found in riverbeds, gravel pits, and near volcanic regions like the Lake Superior area and Western United States.
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Epidote
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